热层冷却辐射对负压脉冲的增强反应
Tikemani Bag1, Yasunobu Ogawa2
1National Institute of Polar Research, 10-3, Midori-cho, Tachikawa, Tokyo, 190-8518, Japan. tikemani.bag@nipr.ac.jp.
Scientific reports
|April 26, 2024
概括
在负压冲动后,氧化 (NO) 排放在热层显著增加. 这种由地磁活动驱动的增强,会影响整个磁层-离子层-热层系统.
科学领域:
- 空间物理 空间物理
- 大气科学 大气科学
- 地质物理学 地质物理学
背景情况:
- 氧化 (NO) 5.3微米的排放对于调节热层温度至关重要.
- 负压脉冲显著影响地球的磁层和电离层.
研究的目的:
- 为了研究NO5.3微米排放对负压冲动事件的反应.
- 了解将地磁活动与NO排放变化的机制.
主要方法:
- 使用宽带发射放射测量 (SABER) 卫星观测对大气的探测. 卫星观测.
- 采用开放地理空间通用流通模型 (OpenGGCM),韦默模型和TIMED/SABER数据.
- 从EISCAT Troms雷达和TIEGCM模拟中分析了电场和导电能力.
主要成果:
- 在脉冲后的高度区域观察到NO排放的显著增强.
- 现场调整电流 (FACs) 的强化和向赤道扩张得到确认.
- 增强的朱尔加热和颗粒沉与增加的NO冷却排放有关.
结论:
- 负压脉冲会触发地磁反应,从而增加NO排放.
- 磁层-离子层-热层系统是相互连接的,NO排放起着关键的调节作用.
- 这项研究提供了对高层大气中动态合过程的见解.
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